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dc.contributor.authorHolding, Johnna M.
dc.contributor.authorDuarte, Carlos M.
dc.contributor.authorDelgado-Huertas, Antonio
dc.contributor.authorSoetaert, Karline
dc.contributor.authorVonk, Jorien E.
dc.contributor.authorAgusti, Susana
dc.contributor.authorWassmann, Paul
dc.contributor.authorMiddelburg, Jack J.
dc.date.accessioned2017-04-10T07:49:49Z
dc.date.available2017-04-10T07:49:49Z
dc.date.issued2017-03-27
dc.identifier.citationHolding JM, Duarte CM, Delgado-Huertas A, Soetaert K, Vonk JE, et al. (2017) Autochthonous and allochthonous contributions of organic carbon to microbial food webs in Svalbard fjords. Limnology and Oceanography. Available: http://dx.doi.org/10.1002/lno.10526.
dc.identifier.issn0024-3590
dc.identifier.doi10.1002/lno.10526
dc.identifier.urihttp://hdl.handle.net/10754/623071
dc.description.abstractRising temperatures in the Arctic Ocean are causing sea ice and glaciers to melt at record breaking rates, which has consequences for carbon cycling in the Arctic Ocean that are yet to be fully understood. Microbial carbon cycling is driven by internal processing of in situ produced organic carbon (OC), however recent research suggests that melt water from sea ice and glaciers could introduce an allochthonous source of OC to the microbial food web with ramifications for the metabolic balance of plankton communities. In this study, we characterized autochthonous and allochthonous sources of OC to the Western Svalbard fjord system using stable isotopes of carbon. We quantified δ13C of eukaryotic and prokaryotic planktonic groups using polar lipid-derived fatty acids as biomarkers in addition to measuring δ13C of marine particulate OC and dissolved OC from glacial runoff. δ13C of bacteria (−22.5‰) was higher than that of glacial runoff OC (−28.5‰) and other phytoplankton groups (−24.7 to −29.1‰), which suggests that marine bacteria preferentially use a third source of OC. We present a Bayesian three-source δ13C mixing model whereby ∼ 60% of bacteria carbon is derived from OC in sea ice, and the remaining carbon is derived from autochthonous production and glacial-derived OC. These results suggest that subsidies of OC from melting glaciers will not likely influence microbial carbon cycling in Svalbard fjords in the future and that further research is needed to determine the effects of melting sea ice on microbial carbon cycling in fjord systems and elsewhere in the Arctic Ocean.
dc.description.sponsorshipWe thank the captain and crew of the R/V Helmer Hanssen, J.C. Alonso for nutrient measurements, A. Dorsett for assistance with DOC measurements, Pieter van Rijswijk and Peter van Breugel for assistance with PLFA analysis and measurements, the Royal Netherlands Institute for Sea research (NIOZ) in Yerseke for accommodation, laboratory space, and technical support, and D. van Oevelen for coordinating analyses at NIOZ. This research was supported by the ARCTICMED project funded by the Spanish Ministry of Economy and Inovation (ref. CTM2011-15792-E) and the Netherlands Earth System Science Center. J.H. was supported by a JAE fellowship (CSIC, Spain).
dc.publisherWiley
dc.relation.urlhttp://onlinelibrary.wiley.com/doi/10.1002/lno.10526/full
dc.rightsArchived with thanks to Limnology and Oceanography
dc.titleAutochthonous and allochthonous contributions of organic carbon to microbial food webs in Svalbard fjords
dc.typeArticle
dc.contributor.departmentBiological and Environmental Sciences and Engineering (BESE) Division
dc.contributor.departmentMarine Science Program
dc.contributor.departmentRed Sea Research Center (RSRC)
dc.identifier.journalLimnology and Oceanography
dc.eprint.versionPublisher's Version/PDF
dc.contributor.institutionDepartment of Global Change Research; Instituto Mediterráneo de Estudios Avanzados (CSIC- Univ. Islas Balears); Esporles Spain
dc.contributor.institutionArctic Research Centre, Bioscience, Aarhus University; Aarhus C Denmark
dc.contributor.institutionFaculty of Biosciences; Fisheries and Economics, UiT, The Arctic University of Norway; Tromso, Norway
dc.contributor.institutionLaboratorio de Biogeoquímica de Isótopos Estables, Instituto Andaluz de Ciencias de la Tierra (CSIC-Univ. Granada); Granada Spain
dc.contributor.institutionDepartment of Estuarine and Delta Systems; Royal Netherlands Institute for Sea Research; Yerseke The Netherlands
dc.contributor.institutionFaculty of Earth and Life Science; Department of Earth Sciences, Vrije Universiteit; Amsterdam The Netherlands
dc.contributor.institutionFaculty of Geosciences; Department of Earth Sciences, University of Utrecht; Utrecht The Netherlands
kaust.personDuarte, Carlos M.
kaust.personAgusti, Susana
refterms.dateFOA2018-06-14T05:13:46Z
dc.date.published-online2017-03-27
dc.date.published-print2017-05


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